Carbon and sulphur tracing from soil organic sulphur in plants and soil microorganisms
Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid
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Yn: Soil Biology and Biochemistry, Cyfrol 150, 107971, 01.11.2020.
Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid
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T1 - Carbon and sulphur tracing from soil organic sulphur in plants and soil microorganisms
AU - Ma, Qingxu
AU - Luo, Yu
AU - Wen, Yuan
AU - Hill, Paul W.
AU - Chadwick, David R.
AU - Wu, Lianghuan
AU - Jones, Davey L.
PY - 2020/11/1
Y1 - 2020/11/1
N2 - In soils, cysteine and methionine represent the predominant constituents of the low molecular weight organic S, but their role in plant nutrition and soil S cycling is unclear. Cysteine and methionine uptake by pot-cultivated wheat and oilseed rape and their cycling were evaluated using 14C and 35S labelling. About 0.16%–0.30% of 14C from cysteine and methionine was absorbed by the plants after 6 h, indicating that the plants could utilise organic S, with oilseed rape showing higher ability than wheat to take up intact organic S and its derivative inorganic S. Plants utilised organic S with much lower efficiency than inorganic S because most organic S was decomposed by microorganisms. Nitrogen (N) addition enhanced plant S uptake, as high N uptake stimulates S immobilization. About 28%–33% and 67–71% of 14C from cysteine and methionine, respectively, were retained in the microbial biomass (MB), a much higher proportion of 14C from cysteine was released as 14CO2 from the soil than from methionine. Further, 16%–25% and 61%–72% of 35S from cysteine and methionine, respectively, were retained in the MB, and 35%–42% and 5%–9% were released from it as SO42−. Microbial carbon (C) and S use efficiency for cysteine was lower than for methionine, whereas plants utilised higher amounts of cysteine-derived S as sulphate. The higher microbial utilisation rate of methionine by soil microorganisms, compared with cysteine, may reduce the bioavailability of this compound in the soil solution, and, consequently, its uptake by plants.
AB - In soils, cysteine and methionine represent the predominant constituents of the low molecular weight organic S, but their role in plant nutrition and soil S cycling is unclear. Cysteine and methionine uptake by pot-cultivated wheat and oilseed rape and their cycling were evaluated using 14C and 35S labelling. About 0.16%–0.30% of 14C from cysteine and methionine was absorbed by the plants after 6 h, indicating that the plants could utilise organic S, with oilseed rape showing higher ability than wheat to take up intact organic S and its derivative inorganic S. Plants utilised organic S with much lower efficiency than inorganic S because most organic S was decomposed by microorganisms. Nitrogen (N) addition enhanced plant S uptake, as high N uptake stimulates S immobilization. About 28%–33% and 67–71% of 14C from cysteine and methionine, respectively, were retained in the microbial biomass (MB), a much higher proportion of 14C from cysteine was released as 14CO2 from the soil than from methionine. Further, 16%–25% and 61%–72% of 35S from cysteine and methionine, respectively, were retained in the MB, and 35%–42% and 5%–9% were released from it as SO42−. Microbial carbon (C) and S use efficiency for cysteine was lower than for methionine, whereas plants utilised higher amounts of cysteine-derived S as sulphate. The higher microbial utilisation rate of methionine by soil microorganisms, compared with cysteine, may reduce the bioavailability of this compound in the soil solution, and, consequently, its uptake by plants.
KW - Sulphur cycling
KW - Plant sulphur deficiency
KW - Isotopic labelling
KW - Soil microorganism
KW - Cysteine and methionine
U2 - 10.1016/j.soilbio.2020.107971
DO - 10.1016/j.soilbio.2020.107971
M3 - Article
VL - 150
JO - Soil Biology and Biochemistry
JF - Soil Biology and Biochemistry
SN - 0038-0717
M1 - 107971
ER -